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Predictive Mineralogy

Possible unrecorded species at Pedra da Moura Mine, Touvedo (São Lourenço e Salvador), Ponte da Barca, Viana do Castelo, Portugal

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
GalenaPbS99.99%Arsenopyrite (53.61 %), Bismuthinite (57.89 %), Chalcopyrite (51.07 %), Cosalite (76.90 %), Eskimoite (86.96 %), Galenobismutite (78.34 %), Matildite (84.44 %), Scorodite (50.30 %), Sphalerite (74.68 %)
MitridatiteCa2Fe3+3(PO4)3O2 · 3H2O99.71%Bermanite (58.06 %), Fairfieldite (54.32 %), Frondelite (59.68 %), Reddingite (51.85 %), Robertsite (61.36 %), Stewartite (58.93 %), Strunzite (51.43 %)
CalciteCaCO396.67%Chamosite (60.72 %), Cosalite (54.82 %), Galenobismutite (60.37 %), Matildite (52.70 %)
Heterosite(Fe3+,Mn3+)PO490.92%Frondelite (51.61 %), Robertsite (50.00 %), Stewartite (62.50 %)
LaueiteMn2+Fe3+2(PO4)2(OH)2 · 8H2O84.44%Bermanite (51.61 %), Stewartite (67.86 %)
HematiteFe2O377.51%Berlinite (54.84 %), Chamosite (50.22 %)
PyrrhotiteFe1-xS77.43%Cosalite (51.52 %), Galenobismutite (53.46 %)
ZirconZr(SiO4)75.18%Fairfieldite (70.37 %), Reddingite (55.56 %), Strunzite (54.29 %)
GoldAu63.97%Eskimoite (56.52 %), Galenobismutite (53.92 %)
CassiteriteSnO263.80%Fairfieldite (51.85 %), Purpurite (57.95 %)
SpodumeneLiAlSi2O662.13%Lithiophilite (62.13 %)
UraniniteUO259.25%Fairfieldite (59.26 %)
AlmandineFe2+3Al2(SiO4)354.32%Fairfieldite (54.32 %)
BismuthBi50.69%Galenobismutite (50.69 %)

Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)


Predicting paragenetic modes of deposit

Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.

Paragenetic ModeScore
34 : Complex granite pegmatites

Unique: Lithiophilite, Manganosegelerite, Triphylite, Zwieselite
151
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Cosalite, Eskimoite, Matildite
100
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]24
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]17
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)10
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)5
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]3
21 : Chemically precipitated carbonate, phosphate, iron formations2
31 : Thermally altered carbonate, phosphate, and iron formations2
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]2
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)2
24 : Authigenic minerals in terrestrial sediments (see also #17)2